Liquid flow in a permeable earth formation



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M. K. ABDO LIQUID FLOW IN A PERMEABLE EARTH FORMATION Original Filed March 16, 1964 VISCOSITY p VISCOSITY p QUJBUH WWW 9 Sheets-Sheet 1 SHEAR RATE,. sec" INVENTOR.

MILTON K. ABDO PATENT AGENT Aug. 27, 1968' M. K. ABDO LIQUID FLOW IN A PERMEABLE EARTH FORMATION 9 Sheets-Sheet 2 Original Filed March 16. 1964 6 MEE 555 1968 M. K. ABDO 3,398,792

LIQUID FLOW IN A PERMEABLE EARTH FORMATION Original Filed March 16, 1964 9 Sheets-Sheet 5 VISCOSITY,}J ,cp.

INVENTOR. MILTON K. A800 BY yw Ms PATENT AGENT Aug. 27, 1968 M. K. ABDO LIQUID FLOW IN A PERMEABLE EARTH FORMATION Original Filed March 16, 1964 9 Sheets-Sheet 4 NJO Aug. 27, 1968 M. K. ABDO 3,398,792

LIQUID FLOW IN A PERMEABLE EARTH FORMATION Original Filed March 16, 1964 9 Sheets-Sheet 5 HE J 55. 551m 069 0 9 o o On On O m ALISODSIA 3A|iv13u ssaaxa QQK Aug. 27, 1968 M. K. ABDO LIQUID FLOW IN A PERMEABLE EARTH FORMATION 9 Sheets-Sheet 6 Original Filed March 16, 1964 IOO TEMPERATURE, C

INVENTOR MILTON K. ABDO PATENT AGENT Aug. 27, 1968 M. K. ABDO LIQUID FLOW IN A PERMEABLE EARTH FORMATION 9 Sheets-Sheet 7 Original Filed March 16, 1964 SYMBOL SHEAR RATE, (3, SEC" INVENTOR MlLTON K. ABDO 7 PATENT AGENT M. K. ABDO LIQUID FLOW IN A PERMEABLE EARTH FORMATION Aug. 27, 1968 3,398,792

Original Filed March 16, 1964 9 Sheets-Sheet 8 no SHEAR RATE, e, sEc' 0.15 WT. %YADDITIVE 0.04s WT.

M. K: ABDO 3,398,792

LIQUID FLOW IN A PERMEABLE EARTH FORMATION 9 Sheets-Sheet 9 Aug. 27, 1968 Original Filed March 16, 1964 l l l O I .05 DJ 0.15

WT. ADDITIVE FflG IO INVENTOR MILTON K. ABDO PATENT AGENT Unied S ate Pam I ABSTRACT. on. THE DISCLOSURE This specification discloses a nethod of treating a subterranean formation by passing into and flowing in the formation a liquid which is either positive nonsirnple, shear hardening, or both. In specific embodiments, various'liquids, bothmiscible and immiscible, are employed as flooding liquids and flowed from an injection well with in the formation toward a production well to recover a large .portion of the oil from the subterranean formation.

By the rheological properties of shear hardening and/or positive nons'implicity,theflooding liquids correct for permeability inhomogeneities'a's well as instabilityeifects. Illustrative of the immiscible liquids having the desired rheological properties are aqueous solutions of alkaline soaps of fatty acids with'electrolytepresent where appropriate, aqueous solutions of copper cetyl phenyl ether sulfonate, and aqueous solutions of acid'soap and acid; such as, hex'adecylamidehydrochloride and hydrochloric acid. Illustrative of the miscible liquids having these rheological properties are hydrocarbon solutions of aluminum soaps of fatty acids or of naphthenic acids, or solutions containing at least 2 percent by weight nitrocellulose dissolved in n-butyl acetate.

This is a division of application Ser. No. 351,936, filed Mar. 16,1964.

This invention relates to the flow of a liquid in a permeablelearth formation. More particularly, this invention pertains to recovering oil from subterranean formations. Still more particularly, this invention is directed to. recovering oil-from a subterranean formation byflowing therethrough a flooding liquid.

In various operations for the treatment ofa permeable subterranean formation, a liquidis passed into the formation from a well penetrating the formation. For example, for the treatment vof a subterranean formation to improve recovery of oil thereform, a liquid is. flowed into the formationfroma .well passing from, the surface of the earth to ,the formation. In one such operation, the liquid is flowed intothe formation to displace the formationto a productionwell. v

The oil accumulated in subterranean formations isrecovered-or ,produced therefrom; through wells, calledv production wells, drilledinto the; subterranean formations. Alarge amount of the oil is left in a subterranean formationif produced only by ,primary depletion, i.e., where only. initial formation energyis used to recover the oil. To improve the extentof recovery, supplemental operations,

oil from the often referred to as secondary recovery operations, are used. In the most successfulandrnost widely used supplemental recovery operations, a.fluid, as indicated above, is injected through at least one .well, calledan injection well, andpassed through theformation. Oil is moved through the formation and is produced from a production well or wells thereabout, as the injected fluid passes from the injection well to the production wel ls Two major-types of sweep etficiency-macroscopic or areal sweep efliciency and microscopic sweep efliciencyinfluence the effectiveness of the passage of the injected fluid through the formation.

The first type, the macroscopic or areal sweep efficiency, is most seriously affected 'by the permeability stratification of the subterranean formation and by the difference between the viscosity of the in-situ oil and the injected fluid. In any operation in which a fluid is injected through an injection well into a subterranean formation, permeability stratification is significant. It is most significant in. secondary-recovery operations. By causing a disproportionately large amount of the injected fluid to enter the more permeable zones, it results in premature production of the injected fluid at production wells thereabout. This premature production is referred to as premature breakthrough and is reflected as an increasing ratio of the injected fluid to the oil in the produced fluids. Thus, premature breakthrough can render an otherwise well-engineered recovery project relatively ineifective because of the cost of treating and recycling the injected fluid.

A sharp difierence in viscosity between that of the insitu oil and that of the injected fluid creates a situation referred to as instability when the viscosity of the injected fluid is less than that of the in-situ oil. The less viscous injected fluid tends to develop fingers or bulges which may be caused by a point of minute inhomogeneity in the formation. These fingers grow and travel at a much faster rate than the remainder of the injected fluid and thus also cause premature breakthrough.

Various means have been proposed to avoid premature breakthrough. Selective plugging operations have been taugnt to correct permeability stratification. Viscosity gradation, wherein an intermediate fluid or fluids having a viscosity between that of the injected fluid and that of the in-situ oil is employed, is taught to cure or minimize instability fingering. One method which has been taught to correct both the permeability stratification and the instability fingering involves the use of a thickener in the leading edge of the flooding or displacing liquid comprising one of the injected fluids. Morespecifically, it has been taught to add thickeners to the [leading edge of a waterflood, i.e., a recovery operation where the injected displacing liquid is water.

The second type, the microscopic sweep efliciency, is influenced by the interfacial tension and the contact angle between the injected fluid and the in-situ oil, and the permeability of the formation. Available methods of altering permeability, such as fracturing or acidizing, are of limited benefit. The greater the interfacial tension, the more resistance thedisplacing fluid will encounter in attempting to flush the oil from the more restricted interstices ofvthe formation. To achieve improved microscopic sweep efliciency, it has been taught to add a surfactant to a flooding liquid to decrease the interfacial tension and toalter thecontact angle.

Despite experimental and field use of the foregoing additives and methods, much oil continues to remain in a subterranean formation after the best recovery mechanisms heretofore known have been employed.

Therefore, it is an object of this invention to provide additives and additive systems for solutions used in the treatment of a permeable subterranean formation.

It is a more specific object of this invention to provide additives and additive systems which will enhance the oil recovery capability of a flooding liquid to which they are added.

It is also an object of this invention to provide a floodingliquid tending to even out injection and flow profiles in .a subterranean formation, thus benefiting the distribution patterns of any other fluids injected concurrently, alternately, or subsequently. v I

More particularly, it is an object of the invention to provide a flooding liquid which will increase both the macroscopic and the microscopic sweep efliciencies of a flooding operation.

It is another object of the invention to provide a method of recovering additional oil by passing through a subterranean formation a flooding liquid which will increase both the mascroscopic and microscopic sweep efficiencies of the flooding operation.

It is another object of the invention to provide a method of decreasing the flow of a flooding liquid in more permeable domains relative to flow in less permeable domains of a subterranean formation.

In accordance with the invention, in the treatment of a permeable subterranean formation wherein a liquid is flowed into the formation from an injection well, a positive nonsimple liquid is employed. In a specific aspect of the invention, in the recovery of oil .from a subterranean formation by injecting a flooding liquid through an injection well and into the formation and producing oil from the formation through a production well, a positive nonsimple liquid is employed as the flooding liquid.

The use of the positive nonsimple liquid will provide advantages in formations having permeability stratification. A positive nonsimple liquid is a liquid whose viscosity varies in the same direction as the permeability, k, when it flows in various porous solids at the same nominal shear rate,

within limits. Viscosity of a liquid flowing in a formation or in a core sample therefrom, often called apparent viscosity, is determined from Darcys law as follows:

In these expressions,

k=permeability, in darcies, of the porous solid, formation, orcore sample,

IL=VISCOSitY in centipoises of the liquid,

V=Darcy velocity of the flow of the liquid, or the volume flux rate per unit area, in centimeters per second,

P=pressure in atmospheres, and

X=length, in centimeters, along the linear axis of the pressure gradient.

Thus, at any nominal rate of shear the apparent viscosity of a positive nonsimple liquid will be equal to or higher in a more permeable stratum in a subterranean formation than in a less permeablestratum. Within a certain range of shear rates, the apparent viscosity will be higher in a more permeable stratum. The liquid thus is active in the sense that it adjusts its properties to flow at a rate which is relatively insensitive to permeability of a subterranean formation.

In the practice of the invention, the positive nonsimple liquid employed, as discussed more fully hereinafter, will be a solution of a solute in a solvent. 7

FIGURE 1 is a plot of a typical apparent viscosity response of a nonsimple liquid as a function of shear rate in strata having different average permeabilities, k.

FIGURE 2 is a plot of typical viscosity responses of various kinds of liquids as a function of shear rate.

FIGURE 3 is a plot of excess relative viscosity, defined below, of a positive nonsimple liquid as a function of shear rate.

FIGURE 4 is a plot of the viscosity response of a positive nonsimple liquid to shear rate in a viscometer and in two core samples having different permeabilities.

FIGURE 5 is a plot of flow rate of several liquids through a model comprising an unconsolidated sand pack as a function of pressure drop.

FIGURE 6 is a plot of the excess relative viscosity of a V -ranked aqueous positive nonsimple liquid as a function of shear rate at various temperatures.

FIGURE 7 is a plot of the activity index, A, defined below, as a function of temperature for a V -ranked liquid.

FIGURE 8 is a plot of viscosity response of a positive nonsimple liquid as a function of shear rate at different pH values.

FIGURE 9 is a plot of the excess relative viscosity of an aqueous positive nonsimple liquid at different additive concentrations as a function of shear rate.

FIGURE 10 is a plot of the activity index, A5, of an aqueous positive nonsimple liquid as a function 'of additive concentration.

Each subterranean formation contains a spectrum of domains of different permeabilities. If more permeable domains predominate in a particular stratum in a formation, the stratum will have a higher average permeability than a stratum where less permeable domains predominate. Typically, a stratum having, for example, an average permeability of 400 millid-arcies will be comprised of a spectrum of domains ranging in permeabilities from 200 to 800 millidarcies.

When injected through an injection well into a subterranean formation, a positive nonsimple liquid tends to even out or compensate for permeability variations because of its own internal flow control mechanism. This internal flow control mechanism operates to increase the apparent viscosity of the liquid in the more permeable domains over that in the less permeable domains within the formation; The internal flow control mechanism is particularly effective where there are strata having different average permeabilities. Thus, the injected positive nonsimple liquid tends to flow at a more nearly uniform velocity in all strata in the subterranean formation regardless of the permeability therein. As a result, more oil is recovered before breakthrough of the flooding liquid.

Typical behavior of a positive nonsimple liquid is shown in FIGURE 1 where the apparent viscosity, [.L, of the liquid flowing in permeable strata is plotted versus the nominal shear rate of the liquid in the strata, as calculated from the velocity, V, divided by the square root of the permeability, k In this figure, the permeability of the stratum for curve K is higher than the permeability of the stratum for curve K .Similarly, the permeability of the stratum for curve K is higher than the permeability of the stratum for curve K The permeability of the stratum for curve K is also higher than the permeability -of the stratum for curve K The better a positive nonsimple liquid performs as .a flooding liquid, the greater will be the area, typified by areaA in thefigure, under the curve representing its viscosity as a function of shear rate in a stratum having a particular permeability, k.

The, area A gives a comparative evaluation ofthe integral V I Md ln a=viscosity V V/k =nominal shear rate,

V=velocity,

k=per meability,

r radius from the injection well at which the shear rate is low enough 'to sustain a positive viscosity variation (for evaluating the integral it can be assumed equal to the radius of 'the injection well),

r =radius from the injection well at which the shear rate is high enough to develop a positive viscosity variation (for evaluating the integral it can be assumed equal to one-half the distance to the production Well), and

A=activity of the positive nonsimple liquid.

Positive nonsimple liquids having a greater activity, i.e., a greater value of A, begin to show a positive viscosity variation at lower rates of shear and have higher viscosities at all rates of shear within the limits of eifectiveness than do less active liquids.

If a n'onsimple liquid develops a lower viscosity when it flows in more permeable strata than when it flows in parallel-connected flow in less permeable strata, it is a negative nonsimple liquid in the sense of this invention. If the apparent viscosity of a liquid does not change when it flows in parallel through strata having varying permeabilities, the liquid is a simple liquid.

Insofar as is presently known, all liquids which are positive nonsimple liquids have a range of shear rates in which increasing shear rate increases their apparent viscosity. This range is referred to as the shear hardening or shear thickening region. However, although shear hardenin is-a sufiicient condition to render a liquid effective in the method of the invention, it is not a necessary condition.

Shear hardening, or shear thickening, is a fairly unusual rhoeological property. It has been observed in some past experimental work with non-Newtonian liquids and has been variously reported, not always correctly, in terms of the liquids being dilatant, rheopetic, or negatively thixotropic. Whether any non-Newtonian liquid exhibits the property of shear hardening or not can be determined by its viscosity (ratio of stress to rate of shear measured at the wall of the viscometer container) at given rates of shear measured on a viscometer, such as the Couette or Brookfield viscometers. Typical curves are illustrated in FIGURE 2.

Referring to FIGURE 2, a liquid which exhibits the rheological property of shear hardening or shear thickening will have a viscosity curve similar to curve 10. The viscosity will increase at increasing rates of shear, within limits, above the constant viscosity of a Newtonian liquid having the same initial viscosity, e.g., curve 11. There will be a finite shear rate at which this viscosity will pass through a maximum. Beyond this, a shear rate increase will bring about a decrease in viscosity, i.e., curve will eventually return to curve 11 at some rate of shear. Every liquid which exhibits a region of shear hardening is useful in the method of the invention. However, those liquids which also are positive nonsimple liquids are more efiective since they compensate for continuously varying permeability. They also compensate more effectively over I will exhibit a viscosity which is lower at high rates of shear than a Newtonian fluid having the same initial viscosity, e.g., curve 13.

Flow experiments, for example, employing long core samples, in which apparent viscosity can be measured as a, ,function of shear rate are very time consuming. Fortunately, the viscometers,. such as the- Couette or Brookfieldviscometers, having concentric cylinders afiord a good correlation with behavior in a subterranean formation. Liquids which show an increase in viscosity with larger gap sizes on the viscometer at certain given rates of shear are useful inthe method of the invention. The gap size in such a viscometer is simply the distance separating the concentric cylinder walls immersed in the liquid. A typical curve for a solution is shown in FIG- URE 3. In the figure, curve 16 is a plot of the excess relative viscosity, i.e., the viscosity of the solution above that of the solvent divided by that of the solvent to provide a dimensionless number, versus the shear rate at a gap size of 0.1232 centimeter. Curve 17 is a plot of the excess relative viscosity of the same solution using a gap size of 0.0790 centimeter. Thus, the solution is a positive nonsimple liquid. The area A, 1e.g., under curve 16, affords an index of the activity of the liquid, i.e., its efiicacy as a flooding liquid for recovering oil. It is particularly indicative of the liquids internal flow control capability, i.e., the ability of the liquid to flow at a more nearly uniform velocity in all strata in a formation regardless of the permeability of each respective stratum. This area, A, is an evaluation of the integral where =shear rate in secf =minimum rate of shear at which a positive viscosity variation is developed; can be assumed to be 0 herein,

=maximum rate of shear at which a positive viscosity variation is sustained; can be assumed to be oo-for liquids where i /a returns to 0,

a=viscosity of the solution in centipoises (for evaluations of activity indices herein),

a =viscosity of the solvent in centipoises, and

A-=activity index.

This integral is empirically analogous to the integral 11 V H E I] and is indicative of the relative efficacy of a liquid as a flooding liquid.

It becomes convenient to give subjective estimates of the area, A, instead of planimetering each curve for an indication of effectiveness of a liquid when many liquids are tested. Such subjective estimates can best be described in terms of rank or symbols representative of the efiicacy of the liquid being evaluated. Approximate quantitative values for the areas can be ascribed to the rank or symbols. The data included herein is reported using the symbols. Table I below explains the symbols. It gives the approximate evaluation of .the integral, A, i.e., the area under the curve representing its excess relative viscosity as a function of shear rate'using a Couette device, the UL. adapter of a Brookfield Model LVT Synchro- Lectric Viscometer having variable revolutions per minute, and using a gap size of 0.1232 centimeter between concentric cylinders having radii of 1.2573 and 1.3805 centimeters. 'It also gives the relative eflicacy of: the liquids as flooding liquids, i.e., how much more effective is the solution than the solvent. Liquids having a rank above X are active and are useful in the method of the invention. a

7 TABLE I Bank or e; t V Symbol d ln e Effective i I Not.

1-3 Slightly. 440 1 Moderately. ll-20 Very.

21-50 Highly.

50 Extremely. I

Typical behavior of a positi'ye nonsimple liquid when used as a flooding liquid is shown in the following example. A dilute aqueous solution which was a positive nonsimple liquid having a ranking symbolized by V gave an integrated area, A, under its curve 16, as shown in FIGURE 3, of 43. It was highly effective in increasing the recovery of oil at breakthrough from a core sample over that of water alone. It was used in displacing Sovasol, a paraflinic hydrocarbon cut just below kerosine in its boiling point range, from a core sample composed of crushed quartz consolidated with calcium alumi'nate. The core sample was designated Model C and had a diameter of 1.21 centimeters, a length of 113.03 centimeters, a pore volume of 52.5 milliliters, a porosity of 40.35 percent, and a permeability of 1.34 darcies. Model C was saturated with Sovasol to 100 percent saturation. The Sovasol represented the oil phase. It is hereafter referred to as oil in connection with the core sample models. The oil was flooded from the core sample using water alone and the core sample was again resaturated to 100 percent oil saturation. The oil was then flushed from the core sample using the dilute aqueous positive nonsimple liquid. Duplicating runs were made to verify the results. To reduce the residual oil saturation to 53 percent required approximately 2.84 pore volumes of water and entailed production at a water-oil ratio of approximately 61. By contrast, 1.47 pore volumes of the dilute aqueous positive nonsimple liquid reduced the residual oil saturation to 53 percent, entailing a solutionoil ratio of only 21.

The high degree of effectiveness of the positive nonsimple liquid is shown more clearly in a model simulating a formation having noncommunicating strata of different average per-meabilities. Two core samples having different permeabilities were connected in parallel. Specifically, the above-described Model C was connected in parallel with a Model U, a core sample of unconsolidated highly angular crushed quartz. Model U had a diameter of 1.306 centimeters, a length of 120.6 5 centimeters, a pore volume of 70 milliliters, a porosity of 44 percent, and a permeability of 30.4 darcies. This Model C and Model U in parallel is referred to as a Stratified model or Model S. With Model C and Model U saturated to 100 percent with oil and the oil displaced with water, the water broke through Model U when it had displaced only 4.76 percent of the pore volume of Model C. When resaturated with oil and the displacement repeated using the dilute aqueous solution comprising a positive nonsimple liquid, 34.1 percent of the pore volume of Model C was displaced before the solution broke through Model U.

An M-ranked positive nonsimple liquid is less effective, as the activity index indicates. When oil is displaced from the Model S in the same laboratory experiment, only 18.1 percent pore volume is displaced from Model C before breakthrough in the parallel-connected Model U. While this percentage is appreciably greater than the 4.76 percent realizable by waterflood alone, it is less than the-34.1 percent achieved bythe v -ranked positive nonsimple liquid.

The relative activity of the positive nonsimple liquids is also illustrated by flow behavior in the Model U and -Model C. The actual flow through each model was measured under a AP of 0.08 atmosphere. The flow from Model C was multiplied by (permeability of Model U permeability of Model C son. A V -ranked liquid flowed at an actual rate of 6.4 cubic centimeters per hour in Model U andat a comparative or permeability-corrected rate of 40.9 cubic centimeters per hour in the less permeable Model C, with the AP of-0.08 atmosphere. An M-ranked liquid flowed at an actual rate of 32 cubic centimeters per hour inModel U. and at a comparative rate of cubic centimeters per hour in Model C, with the AP of 0.08 atmosphere. The V -ranked liquid corrects by more than sixfold, while the M-rankedliquid corrects by onlyabout threefold for permeability variation. The activity of a positive nonsimple liquid, indicated by viscometer data, is further illustrated in FIGURE 4. Therein the viscosity variation of the liquid with shear rate in a Couette viscometer and in porous solids, such as consolidated core samples, is plotted. Curve 20 is a plot of the viscosity measured in a Couette device (the U.L. adapter of a Brookfield Model LVT Synchro- Lectric viscometer having variable revolutions per minute). Curve 20 shoWsa region of shear hardening. Curve 21 is a plot of the viscosity measured in a core sample having a permeability of 410 millidarcies. Curve 22 is a plot of viscosity measured in a core sample having a permeability of 4160 millidarcies. The positive nonsimple liquid thus exhibits a dramatic increase in its apparent viscosity in the more permeable core sample. Hence, the liquid flows much less readily in zones of higher per meability than in zones of lower permeability. l

The decrease in flow of a positive nonsimple liquid in more permeable channels with certain pressure drops is compared with that of water in FIGURE 5. Thereimthe flow rate, Q, in cubic centimeters per hour of various liquids, i.e., solutions of additives or combinations of additives, hereinafter called systems, with their symbols designating their flooding effectiveness, through Model U is plotted as a function of the pressure drop, AP, in atmospheres across the model. Those of the liquids which are not positive nonsimple liquids, i.e., are simple liquids, denoted by symbol X, plot a straight line. Thus, even though the systems may be thickeners, the liquids exhibit the same flow characteristics as water. Such simple liquids decrease .their flow rates proportionally in all strata regardless of permeability. They do not exhibit sensitivity to gap size in the Brookfield viscometer, and they do not cause a proportionallygreater flow rate in less permeable strata. Conversely, the positive nonsimple liquids plot a curved line, exhibiting flow characteristics very different from water. Practically, they reduce their flow rates much more dramatically in the more permeable strata than in the less permeable strata. A measure ofthe efficacy of the liquid as a flooding liquid is the Q at which its plot begins to curve away from the water plot. Any positive nonsimple liquid which curves away from the water plot in the manner illustrated will tend go exen out the injection and flow profile of a flooding rqui .a

Most of the additives for flooding liquids previously suggested inthe prior art are thickeners. The liquids containing these thickeners arenot positive nonsimple liquids, but are simple liquids. Many such thickeners exhibit the property of shear thinning, however. When these thickeners are added to the leading edge of ,a flooding liquidptheviscosity gradation ratio may be improved. However, the problem of permeability stratification is not solved by a simple liquid exhibiting shear thinning.

cific circumstances not taught by the prior art wherein the desired properties can be induced. Where theseproperties can be induced into a flooding liquid, an increased recovery is effected in flooding experiments. Some positive nonsimple liquids have a lowered interfacial tension between themselves and the in-situ oil. Others achieve relatively the same additional recovery of oil at breakthrough without nearly as substantial a reduction in intorfacial tension. Thus, lowered interfacial tension is not the primary mechanism responsible for the activity of the positive nonsimple liquids of the invention.

The following is a detailed description of positive nonsimple liquids for use as active flooding liquids and the liquids are divided into two types. The first type is immiscible flooding liquids, particularly aqueous solutions. The second type is miscible flooding liquids, particularly hydrocarbon solutions.

Immiscible flooding liquid Water is .the most commonly used immiscible flooding liquid. Water, as used herein, means the flooding liquid commonly used in waterfloods. ,It includes common oil field brines and commonly available dilute aqueous solutions, such as surface water. The following additives for water are discussed from the standpoint of being added to at least a part of the floodwater to induce the internal flow control capability by converting at least a portion of the Water to a positive nonsimple liquid; more specifically, to a positive nonsimple liquid having the rheological property of shear hardening and being useful in the method of the invention. In the various embodiments described, specific compounds or chemicals are disclosed as being added to the flooding water to obtain the desired positive nonsimple liquid. It will be readily apparent that the addition, or end result, can also be accomplished by effecting any suitable chemical reaction or ion exchange, e.g., by adding a particular baseand reacting it with a particular acid to form directly in the aqueous solution the specific chemicals disclosed. The resulting solutions will be the same as those described in the embodiments and are within the scope of this invention. These positive nonsimple liquids demonstratean activity beyond that of mere water or thickened water.

The particular additive system may be added to only a portion of the water to create a slug or slugs of a positive nonsimple liquid having a volume of from 0.1 to 30 percent, preferably 1 to percent, of the hydrocarbon pore volume of the formation. The slugs of positive nonsimple liquid are injected through the injection well and passed into the formation. Such slugs may be injected once or alternately with larger volumes of untreated water between alternate slugs to achieve the desired recovery :of oil from the subteranean formation. Obviously, water having lower concentrations of additives and hence less activity may be used between alternate slugs instead of untreated water. Each treated slug tends to even out the flow, to alter the pressure gradients, and more nearly to compensate for permeability stratification. Hence, the greater the number of treated slugs, the more effective will be the flood. Obviously, greater recovery of oil will be obtained from a subterranean formation if the entire flooding liquid is converted to a positive nonsimple liquid. This is, of course, more expensive and the particular formation will dictate the economics of the amount and frequency of the slugs which are to be injected, ranging from only one slug to treating all of the flooding water.

Several of the additives and additive systems which follow comprise-soap systems. These systems in water are referred to herein as solutions since the resulting clear liquid flows into permeable core samples without any loss of additive by filtering action.

The soap systems are divided into two types-saturated soaps and unsaturated soaps. The unsaturated soap systems require more additive to form a positive nonsimple liquid. However, they are more soluble and tolerate higher concentrations of sodium chloride than do the saturated soap systems. The saturated soap systems are useful in formations having higher temperatures, as illustrated by data for each embodiment. Saturated as employed herein means that the carbon chain in the soap is saturated with hydrogen atoms. Typical examples are the stearates. and palmitates. Unsaturated is used herein to denote soaps having carbon chains which are not saturated with hydrogen atoms, e.g., the oleates. Theentire family of soap systems can be described generically under a generalized formula as shown below:

19. and

]b where X is alkali metal, such as potassium and sodium; ammonium; amine; and alkanolamine ions;

A is oleate, palmitate, elaidate, and stearate;

Y is potassium, sodium, and ammonium;

B is a halide;

C is hydroxide and carbonate;

a is 0 to 5 percent by weight; and

b is 0 to that sufiicient to give a pH greater than 7.

The alkaline soaps, i.e., the alkali metal, ammonium and amine soap systems, form alkaline aqueous solutions in neutral water. Sufficient quantity of the soap system can be added to form positive nonsimple liquids without the addition of caustic except where (l) the water has a pH less than about 7, and (2) the solution must have a pH greater than about 8.5 to be a positive nonsimple liquid. Under such conditions, the water may not dissolve enough of the alkaline soap system to raise the pH the required amount. In any event, the pH of the soap solution is more easily and economically adjusted to the desired range by adding caustic rather than by adding extra quantities of the alkaline soap. By caustic is meant the alkali metal hydroxides or carbonates. Preferably, sodium hydroxide or sodium carbonate is employed. Suitable caustic also includes ammonium hydroxide, NH OH, although it causes an ion exchange as described below. Sodium carbonate is particularly useful because it tends to give a buffered pH in the desired range even when used in excess of the required amount.

Each embodiment hereinafter is described in terms of sufficient caustic to give a desired pH range, It will be understood, however, that caustic will not be required if the pH of the solution resulting from admixture of the water and the compound (X) (A) is within the range desired. On the other hand, as indicated above, the addition of caustic is preferred from the standpoint of economy.

In general, the soap systems are susceptible to ion exchange and possible precipitation with divalent ions, such as calcium or magnesium, when in contact therewith. Hence, in using these systems, it is preferable to flow a ring of water in advance of the treated flooding water. The ring of water will build up a bank and miscibly displace the solution in the formation containing the divalent ions, thus reducing the tendency to precipitate the divalent soaps. As an additional safeguard, a chelating or seques- 11?] tering' agent, such as tetrasodiumsalt of'ethylene diamine tetraacetic acid, sold commerciallyas sodium Versenate; or sodium phosphate glass, commonly =called sodium hexametaphosphateand sold commercially asCalgon, can be added to thesolution containing the soap-system in an am-ount from 0.1 to 1.5 percent by weight to chelate the divalent ions, particularly calcium. Higher'percentages of agent may be used in the absence of sodium chloride. More than 1.5: percent by weight of the agent should be avoided where relatively high percentages, e.g., 3.5 to 5 percent by Weight, of sodium chloride are present since the resulting flooding liquid is not'a positive nonsimple liquid, nor does it exhibit the property ofshear hardening. Alternatively, the chelating or sequestering agent maybe added to the water injected'into the formation ahead-of the positivennsimple.liquid; The efficacy of thepositivenonsimple liquid for-med by the aqueous solution is very much dependenton--.tl1e temperature andpH of the solution and its environment.

The temperatureof the formationis a-dominant factor in'the selection-of the positive nonsimple liquid to be used-as' flooding liquidsA typical temperature effectcan be seen in FIGURE 6. Therein, the :excess relative viscosity of a system for use in the invention, as hereinafter more fully disclosed, is plotted against shear rate at various temperatures. This system provides a particularly effective positive nonsimple liquid as can be seen from the value of the integral plotted as the activity index, A, in FIGURE 7. By knowing the reservoir temperature and selecting a particular additive system whose optimum response is at that temperature, its efficacy can be vastly improved, as illustrated in FIGURE 7. Therein, the activity index of the particular fluid is about 500, at 20 C. while it is down to approximately 50 at 45 C. The lower the temperature, the more effective will be the positive nonsimple liquid unless the additive will precipitate from the solution. Such precipitation can be observed, first, by the solution becoming opalescent and, subsequently, by the actual formation of the precipitate. The temperature is included in the following tables showingthe efficacy of the various additives in aqueous solutions. I

. As mentioned, the pH within the formation, and its soluble salts, also influence the selection of the positive nonsimple liquid. A typical case of optimizing theqpH response for an additive to be used in an aqueuos solu+ tion is shown in FIGURE 8. In each embodiment .hereafter described, a range of pH is given. An optimum pH will exist near the center of the range except as noted; The eflicacy of the additive, both for inducing the charac'ter'istics of positive nonsimplicity and shear hardening and fo'r improving the recovery of oil, is greatly improved .at' this optimum pH. The viscosity response of one of these typical aqueous positive nonsimple liquidsto varying rates of shear at various pHs is shown in FIGURE 8. The particular solution was another system for use in the invention as more fully disclosed-herein after. Varying amounts of sodium hydroxide were added to different. portions-10f thissolutioni and-the abovedescribed Brookfield Synchro-Lectric Viscometer, Model LVT, was used to measure :the viscosity responsepThe area under the curve'in-F'IGURE 8 does not measure exactly the same integral as the previously described area A in FIGURE 3.-. However,.-it is closely analogous. At the optimum pH-the area is very considerably increased and the effectiveness of the positive nonsimple liquid is equally increased =at-thisoptimurn pH.when used to displace oil from a stratified subsurface formation.

. Theconcentration:of'theadditive can alsobe varied to tailor a positive nonsimple liquid which-is optimum for .the particular subterranean formation. In -general,=.the greater the concentration, the more 'activewill'be the re.- sulting positive nonsimple liquid This can be seen in FIGURE 9 wherein theexcess relative .viscosity of a positive nonsimple liquid is plotted versus the. shear rateiat different concentrations of: the additiVeLaFIGURE 10 shows the activity index, A'.,-.versus the weight percent of the additivein the positive nonsimple liquid. The activity index; A', increases from approximately 25 at 0.045 percent to approximately 400 at 0.15 percent. Increasing .the concentration increases the viscosityv v In one embodimentof the invention, a positive nonsimple liquid is created by forming a dilute aqueous solution having therein an effective concentration of from 0.1 to 1 percent by weight sodium oleate and .1: to-5 percent by Weight sodium chloride. The solution may also contain sufficient caustic to give apH between 7.5 and 12. Sodium hydroxide can be added tothe 'fioodwater along with the sodium oleatein amounts up to about-0.5 weight percent. Sodium -o1eate-withsodium chloride alone. is alkaline; and for certain formations, Water withthese additives may be used-without the addition of caustic.

.A listing of systems whichare. positive nonsimple liquids,.i.e., have the propertyof internal flow control and shear: hardening, is given in Table II. When percent is used in any table, it refers to Weight-percent.

. Asillustratedin-Table II, the upper temperature limit at which theaqueous solution is a positive nonsimple liquid can-ibe .-.exten-ded by increasing the amount 'of sodium chloride, in, the aqueous solution. For example, in System 1, the range of. maximumtemperatures which can be; encountered -in theformation' and still give the imr proved'oil recovery lies betweene25f :and 50". G. with an optimum-temperature being about.30?' C. If the amount of..sodium.-chloride .is, increased-from. 1' to 3-percent as shown by System. 3, ,therange .ofmaximum temperature of the formation is extended from 83 to about 88 C., with .anoptimumofabout 84 C=,.The temperatures given in. Table II, are. ranges of maximum temperatures. At lower temperatures :such as found in formations, the. solutron remains active...Tailoringa specific'waterfloodadditive for a specific formation can beiaccomplished. For example, in System 8,, a lvpercent sodium oleate is added along with 4.5 weight per-cent sodium chloride and about 0.05 weight percent sodium hydroxide togive a positive nonsimple liquid useful as a flooding liquid up to amaximum temperature range of from, 76.to.91. C.

- TABLEZII Water, wt. Sodium Sodium Sodium Tem er System N0. l Percent Wt. V Chloride ydroxide. tux}; a I

4 Percent Percent Wt. Percent Range, ture, C. i v v 1' a 0.10 30-75 -1 3.5 0.10 40-85 1 4 0.10 was TABLE LIL-SODIUM OLEATE SYSTEMS System Na Oleate, NaOH, Wt. NaCl, Wt. Na Versenate, Mols Na+ No. Wt. Percent Percent Percent Wt. Percent T., 0. Rank I v Mols Na Oleate 1'. 0 2. 01 0 10. 29 Va 1. 0 0. 2. 01 0 10. 5 55 V 1.0 0 3.01 0 15. 7 83 V 0. 1 0. 429 2.01 0 137. 1- 29 V2 0. 2 0.102 3. O2 0 82. 5 30 V 0. 2 0. 102 4. 02 0 108. 5 51 X 0. 2 0. 858 4. 02 0 137. 3 75 X 0. 5 0. 766. 3. 00 0 42. 9 61 V 0. '5 0. 766 3. 56 0 48. 7 80 M 0. 79 0.766 3. 56 0 30. 8 00 M 1.0 0. 05 y 3. 04 0 16.2 30 V; 1. 0 0. 05 4. 01 0 21. 3 44 V2 1. 0 0. 05- 4. 52 0 23. 9 76 V2 1. 0 0. 106 3. 01 0 16.5 30 Va 1. 0 0. 106 3. 50 0 19. 0 40 V: 1. 0 0. 106 4.02 0 21. 7 50 V 1. 1 0. 766 3. 56 0 22. 1 85 M 1. 0 0. 10 3. 01 0.99 17. 5 33 V 1.0 0. 10 3. 01 1.51 18.0 34 V 1.0 0. 66 3. 01 1.51 22. 3 80 V 1. 0 0. 66 3. 49 1. 51 24.8 91 X The foregoing is illustrated in Table III. Therein, Sys- 0.08 percent ammonia in the System 41. To obtain pretems 22, 23, and 37 are not active, primarily because of cision, the ammonia which is reported herein was added high salt content. Elevated temperatures are necessary in aqueous solution. where the salt content is so high. However, System 18 il- Refer-ring to Table IV, some solutions are referred to lustrates the decrease in efficacy of a particular system as as opal, meaning they are opalescent. The opalescent the temperature increases above the minimum necessary to solutions can be used in the more permeable formations. achieve an active solution. It decreased from V to V as the In relatively impermeable formations, the opalescent solutemperature increased from 29 to 55 C. A factor of sigtions are not desirable because of their tendency to filter nificance in'these sodium oleate systems is the mol ratio out. It is preferred to use solutions which are clear in of the sodium ions Na to the sodium oleate present. This flooding subterranean formations. Of course, a solution is shown in Table 111. As the mols of sodium per mol of 33 containing a precipitate is undesirable since it tends to sodium oleate increase, the upper limit of temperature at plug all but the most permeable strata.

. TABLE Iv.--s0DIUM 0LEATE-NH3NH4C1 SYSTEMS Na Oleate, NHa, Wt. NH4C1, Wt. Mols NHiCl Descrip- System No. Wt. percent percent percent k pH tion Mols Na Oleate 0. 1 0 0. 02 1. 06 X 7 Opal. 0.1 0.016 0. 02 1.06 x 1. 5 Do. 0. 1 0.062 0. 02 1.06 X a Do. 0. 1 0. 14 0. 02 1.06 V? 10 Clear. 0. 14 0. 259 0 0 X 10. 5 D0. 0. 14 0. 250 0. 025 1. 0 M 10 D0. 0. 14 0. 250 0. 05 2. 0 V 9. 5 D0. 0. 14 0. 51 0. 05 2. 0 V 10. 5 Do. 0. 14 0. 51 0. 221 8. 84 v 10 Opal. 0. 14 0. 613 0. 221 s. 84 M 10. 5 Do. 0.14 0. 729 0.221 8. 84 V2 10. 5 Do.

No, 46:V to M in 5 days. which the sodium oleate solution is apositive nonsimple liquid decreases. In another embodiment of the invention, a positive non- Ammonium ions can be added to these dilute solutions slmple liquid is created by forming a dilute aqueous soluof sodium oleate to eifect a conversion to ammonium tion having therein an eifective concentration of from 0.05

oleate systems which are described in more detail later. to 1 percent by weight potassium oleate and 2 to 5 percent This conversion is set forth in Table IV. System 40, for 50 by weight or more potassium chloride. The solution may example, is not a positive 'nonsimple liquid, while System also contain sufiicient caustic to give a pH greater than 7 41 is very effective. The difference is simply an additional and less than 13.

TABLE V.POTASSIUM OLEATE SYSTEMS 'System Potassium Potassium Potassium Tem Water p. No. Wt. Percent Oleate, Hydroxide, Chloride, 0. Rank Wt. Percent Wt. Percent Wt. Percent Upper temperature limit of activity not determined.

TABLE VL-POTASSIUM OLEATE SYSTEMS AT 25 0.

System No. KOleate, KOH,wt. K01, wt. Rank pH Description wt. percent percent percent 0. 81 2. 10 X 11 Clear. 1. 53 1. 98 X 11 Do. 3. 09 1. 70 X 11 D0. 5. 12 1. 35 X 11 D0. 4. 54 0. 58 X 11 Do. 4. 52 1.00 X 11 D0. 4. 1. 08 X 11 D0. 4. 55 1. 13 X 11 D0. 4. 54 1. 20 X 11 D0. 4. 53 1. 25 X 11 Do. 4. 50 1. 41 X 11 D0. 0. 2 0. 05 S 9 D0. 0. 2 0. 05 M 9 Do. 0. 2 0. 05 V 9 D0. 0. 2 0. 05 V4 9 Clear, viscous.

No. 67: V; to S, 8 days old.

15 Table V illustrates that increasing amounts of potassium chloride in the alkaline potassium oleate solution achieves better recovery. Table VI shows.oth er systems which are relatively inefiective in increasing the recovery.

of oil over that of waterflood, as shown by rank of'X.

In another embodiment of the invention, a positive nonsi mple liquid is created by forrfning adilute aqueous solution having therein an effective concentration of from 0.001 to 1 percent by weight, preferably 0,01 to 0.1 percent :by weight, sodium-palmitate or sodium stearate, and 0.5 to 5 percent by weight sodiumchloride. The solution may also contain sufiicient caustic to give a pH above 7.

Table VII illustrates in Systems 68 through 72 concentrations of sodium palmitate, sodium chloride, and sodium hydroxide which will create an aqueous solution which will have the desired properties up to a relatively high temperature, e.g., 75 C. or higher. Table VI-I also shows other systems and their respective rank. The temperatures set forth in Table V'II are the minimum. tem-. penaturesatwhich the solutions .become clean. The sodium stearate systems are-equally as .efiective as, and behave in a manner very similar. to, the sodium pal: mitate systems. i

- TABLE VIL-SODIUM-PALMITATESYSTEMS- cent by weight, a mmon1um...s t1earate o v I mitate and an excess of ammonium ion. By exces ammonium ion is meant NI-11+ 5'1" addition to 531515051511 soap added. To achieve the excess ammonium ion, ammonia or ammonium hydroxidein an amount from 0.05 to 0.4 percent byfw 'eight is added. Table YIII illustrates that the ammonium palmitat'e systems achieve activity without the presence of ammonium chloride or sodium chloride, although the preseiiee of these salts does noft diminish the activity obtainable therewith:

The ammonium stearate systems areifsumm-arized Table I-X. The sodium chloride ion will extend the maxi- 15 mum operable temperature, hfence the commonly avail} able oil field flooding brines' extend the Qrange of use} I System No.

' pfi" Description Wt. Percent .Percent "Percent as";ee'esaifisssssassaseseee gaxaafma asx zxaxaaaaaw Soap not dispensed at 0., minimum T for dispersion is initial value listed.

In another embodiment of the invention, a positive nium palmitate or ammonium steanate systems in formanonsirr'iple liquid is created by forming a dilute aqe efis tiohs containing 'divalent ions.

TABLEvnL- 'iimmNIUM PALMITA'IE SYSTEMS sytsrtem NH4 Palniitate, Ammonia. h ll TLC],

N a0], Operable Optimum o. Wt. percent Wt. percent; Wt. percent Wt. percent Temp .C Temp., 0. Rank ange,

0. 02 0. 98 0 0 40-42 41 S 0. 02 1. 23 0 0 42-44 42 M 0. 02 1. 62 '0 -0 39-60 Va 0. 02 2. 12 0 0 38-58 42' V 0. 02 2. 57 0v 0 38-52 39 V: 0.02 3. 93 0, 0 37-53 38 V2 0. 12 0. 98 0 0 45-50 45 V 0. 12 3. 93 0 0 47-48 47 S 0. 21 1. 27 0 0 44-47 44 V 0. 02 0. 98 0.2 0 45-58 46 V 0. 10 2. 63 0.5 0 35-63 48 V3 0. 02 0. 98 0. -2 0.5 49-58 49 Va 0. 02 0. 98 0.2 1. 0 54-57 54 0. 02 0. 98 0.38 0. 5 43-52 44 V 0.12 ...3..93 0 1. 0 X

From ammonium Hydroxide reagent 0t specific gravity of 0.89 and containing 29% ammonia.

System No. N H4 Stearate, NHa', NaCl, '1., 0. Rank pH Description Wt. Percent Wt. Percent Wt. Percent 109 0.15 1.28 25 X 10.5 Preclpltate.

50 V Do. 55 S Do.

110 0.15 1.28 1.0 25 X 10.5 Preclpltate.

53 V at. 55 S Do;

111 0. 1. 28 2. 0 25 X Preclpitate.

67 M Clear. 68 8 Do.

' From N'HiOH of specific gravity of 0.89 and containing 29% ammonia.

In another embodiment of the invention, a positive nonsimple liquid is created by forming a dilute aqueous solution having therein an effective concentration of from 0.05 to 0.5 percent by weight ammonium elaidate and an from 31 to 50 C. with the optimum at about 43 C.

The optimum pH for the ammonium elaidate additive is approximately 10. It must be on the alkaline side, i.e., have a pH greater than 7.

In another embodiment of the invention, a positive nonsimple liquid is created by forming a dilute aqueous solution having therein an effective concentration of from 0.1 to 0.5 percent by weight ammonium oleate and ammonium hydroxide. Suflicient ammonium hydroxide may be employed to obtain a solution having a pH between about 9.5 and 11. Alternatively, sodium carbonate may be 35 cent, achieving an oleate solution-oil ratio of only 21 whereas a water-oil ratio of 61 was necessary to achieve the same reduction in residual oil. I

The properties of an ammonium oleate-ammonia system are summarized in Table X. The pH of the solution must be about 10 before the ammonium oleate'ammonia solutions become positive nonsimple liquids. The pH must be about 10.5 before all of the ammonium oleate is dissolved. Hence, some of these systems have to be filtered before being used in most subterranean formations. Increasing the ratio of mols of ammonia to mols of ammonium oleate within a range of about fiftyfold increases the efficacy of the resulting positive nonsimple liquid. Because of the low dissociation constant, the mols of ammonium ion to ammonium oleate increases only about sevenfold. The data in Table X also indicates that a decreasing amount of excess ammonium ion is necessary to produce a positive nonsimple fluid as the concentration of ammonium oleate increases.

TABLE X.AMMONIUM OLEATE, AMMONIA SYSTEMS System NHI Oleate, NHZ, Wt.

No. Wt. percent percent pH Description Mols NHi Oleate Mols NH: Oleate 0. 0046 0. 84 0. 086 X 7. 5 Preolpltate. 0. 097 17. 4 0. 378 X 10 Do. 0. 159 27. 5 0. 483 M 10. 5 Opel. 0. 173 29. 8 0. 505 M 10. 5 D0. 201 34. 7 0. 541 S 10. 5 Do. 0. 237 40. 9 0. 590 V2 10. 5 Clear. 0. 275 47. 0 0. 636 V: 10. 5 D0. 0. 276 47. 7 0. 637 Va 10. 5 Do. 0. 018 1. 4 0. 061 X 8 Precipitete 0. 07 5. 4 0. 121 X 8. 5 Do. 0. 184 14. 2 0. 195 M 9 D0. 0. 269 20. 8 0. 236 V 10. 5 Clear. 1. 29 100. 0 0. 517 V2 10. 5 Do. 2. 59 200. 0 0. 733 V2 11 Do. 0.026 1.0 0.059 X 8. 5 Precipitate. 0. 46 17. 8 0. 249 V 10 Clear. 3.17 61.0 Y 0. 250 v, p 10. 5 Opal. 0. 24 4.2 0. 062 Va 10 D0.

employed along with the ammonuim hydroxide to obtain the desired pH. In this case, the sodium carbonate reduces the amount of ammonium hydroxide required. Also, the sodium carbonate is useful in affording a buffered pH in the desired range for these ammonim oleate solutions and thus tends to maintain the given pH even in the presence of adverse environment.

The ammonuim oleate and excess ammonium hydroxide systems are particularly effective and preferred because they are easy to use under their optimum conditions. Increasing the concentration of ammonium oelate above approximately 0.12 percent by weight does not increase oil recovery as much as similar increases below that concentration.

The ammonium oleate solution having a concentration of 0.28 percent ammonium oleate, 1.25 percent NH OH,

and a pH of 10.5 was used in the previously described 75 example wherein the oil saturation was reduced to 53 per- The data in Table XI illustrates that relatively large quantities of salt may be present in an ammonium oleateammonia-sodium chloride system without loss of activity. In fact, the sodium chloride within limits increases the efiicacy of the ammonium oleate-ammonia system. Less ammonia is required as the concentration of sodium chloride is increased; therefore, reactivity can be obtained at a lower pH. Table XII shows an increasing efficacy with increasing temperatures in the presence of sodium chloride.

Table XIII illustrates the effect of temperature. System at 25 C. does not increase the oil recovery above that of water by any significant amount. At 48 C., however, it is very highly effective. It is still very effective at 56 C., and slightly effective at 60 C. This is typical of the behavior of these systems. The compositions of the systems canbe varied to obtain a very large temperature range wherein the liquids will remain positive nonsimple liquids and effective in the method of the invention.

TABLE XI.AMMONIUM QLEATE, AMMONIA, SODIUM CHL'Q RIDE SYSTE MS NH Oleate, NH Wt. NaCl, Wt.- Mols NH: Mols NH System No. Wt. percent percent percent w Rank pH Descrlptlon 3 Mols N H Oleate Mols NH. Oleate 0.1 0.0046 0.022 0.84 0.086 X 7. 5 Preclpitate. 0.104 0.159 27. 5 0.483 M 10.5 Opal. 0.104 0.237 0.70 40.9 590 M 10.5 Clear. 0.104 0.237 1.10 40.9 0 590 V2 10.5 Opal. 0.104 0.237 1.33 40.9 0 590 V2 10.5 D0. 1.0 0.238 2.0 2.08 0 002 V3 10 Clear, viscous. 1. 0 0. 238 2. 47 2. 08 0. 062 10 Precipitate. 1.02 0.32 2. 46 5. 51 0. 070 V 10 D0. 1.0 0. 499' 2.47 8.77 0.089 Va 10.5 Clear. 1. 0 1.45 2. 47 25. 0.152 Va 11 Clear, viscous. 0.9 3.17 61.9, 0.250 7 V 10.5v Opal. a

TABLE XIL-AMMONIUM OLEATE, AMMONIA, SODIUM onLo RIDE SYSTEMS NHi Oleate, N11 Mols NH4+ NaCl, System N o. Wt. Percent Wt. Percent Wt. Percent pH T., 0. Rank Description Mols NR4 Oleate Y 25 V3. Opal. 129 1. 0 0. 24 0.062 0 10, 35 V Do,

' 41 S Clear. 25 V3 Clear, viscous. 135 1. 0 0.238 0. 062 2. 0 50 V Do,

- Y 62 S Clear.

TABLE XIIL-TEMPERATURE EFFECTS System NHi Oleate, N11 Wt. NaCl, Wt. T., 0. Rank Description N 0. Wt. percent percent percent 23 V giecipitate.

3 eat viscous. 140 1. 0 1. 45 2. 85 56 v2 Clear:

neutralization product of the reaction between an amine, e.g., ethanolamine, and oleic acid in an alkaline environment. Other amines which may be used to neutralize oleic acid and produce amine oleates which are satisfactory are ethylamine, propylamine, diethylamine, dibutylamine, triethylamine, ethylenediamine, and diethylenetriamine. In

Table XIV. The complex ammonium oleate systems are inactive at temperatures as low as C. in the concentrations tested, but considerable activity may be shown up to as high as 70 C., decreasing somewhat but still useful even at 90 C.

general, the alkyl radicals of the amine contain from 1 to 6 carbon atoms. The amines are used in excess of the stoichiometric amount, thus giving a product which is .alkaline in reaction. The amine oleates which may be 40 used can' be primary, secondary, or tertiary. For example,

TABLE XIV.AMMONIUM OLEATE-AMMONIA-AM MONIUM CHLORIDE-SODIUM CHLORIDESODIUM HYDROXIDE SYSTEMS System No. NH4 Oleate, NHa, NH Cl, NaCl, NaOH, T., 0. Rank Description Wt. percent Wt. percent Wt. percent Wt. percent Wt. percent 25 X Precipitate. V Visctfius, clear.

0. 141 1. 02 0. 56 0. 79 2. 46 0. 75 70 M Clean 85 S Do. 90 S Do. 25 X Precipitate. I X Viscous, precipitate. V Clear, viscous. 142 1. 0 3.17 0.2 2. 47 0.14 V Do. V Do. V Clear. S Do.

- In-another embodiment of the invention, a' positive nonsimple liquid is created by forming a dilute aqueous solution having therein an effective concentration of from 0.01 to 5 percent amine oleates oralkanol amine oleates. These amines are often called substituted ammonium compounds. The resulting binary system is very easy to 60 use as a flooding liquid and is a particularly eflFective and preferred flooding liquid. A typical amine oleate is the 55 secondary butylamine oleate, often called secondary butyl TABLE XV.SEC-BUTYLAMINE (s-BA) OLEATE SYSTEMS, TEMPERATURE VARIATION s-BA Oleate, KOH,Wt. NaCl, Wt. NaOH,Wt. NaVersen-ate Ca++*Wt. T. 0. Rank H Descri ti 11 Wt. Percent Percent Percent Percent Wt. Percent Percent p 0 0.04 0.015 25 V2 9 Clear.- 0.04 0.03 25 M 9.5 Do. 0.06 0.03 25 V 9.5 Do. 0.17 0.015 25 V2 9' Do.

48 V 9 51 S 9 0.44 25 V 9 40 V 9 48 V 9 52 S 9 159 0.44 0.015 25 V 38 V3 45 V 47 S TABLE XV.SEC-BUTYLAMINE (s-BA) OLEATE SYSTEMS, TEMPERATURE VARIATION-Continued System No. s-BA Oleate, KOH, Wt. NaCl, Wt. NaOH, Wt. Na Versenate, Oa++ Wt. T., 0. Rank pH Description Wt. Percent Pare/ant Percent Percent Wt. Percent Percent 5123 a M mmwmmmmmg 0 0 Calcium added as calcium chloride; 

